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Relevance of groundwater interaction with surface water to the eco-hydrology of semi-arid regions

机译:地下水与地表水与半干旱区生态水学的相关性

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The interaction of groundwater with surface water is an important process for maintaining the ecosystem. The process affects the ecology of surface water by sustaining streamflow during periods of low flow, moderates water level fluctuations of groundwater-connected lakes, and maintains wetlands which serve as habitats for a myriad of wildlife. The interaction also helps to stabilize water temperature as well as concentrations of nutrients and other organic/inorganic compounds in water. Thus groundwater interaction with surface water helps to provide thermal refuge for aquatic species in semi-arid regions where temperatures may otherwise rise to levels that may be lethal to these species. With the growing demand for the sustainable management and utilization of natural resources a better understanding of all components of the ecosystem, such as the linkage between groundwater and surface water becomes imperative. This is even more relevant for the semi-arid regions where the impacts of environmental stresses tend to be more pronounced. This paper is the refore intended to review fundamental concepts of the ecohydrology of the interaction of groundwater with surface water, and discuss the relevance of this interaction to the sustainable management of water resources of semi-arid regions.
机译:地表水地下水的相互作用是维持生态系统的一个重要过程。该过程会影响表面的水通过维持期间径流低流量的周期生态,地下水连接湖泊的温和水位的波动,并保持其用作野生动物栖息地无数湿地。的相互作用也有助于稳定的水温以及营养物和水的其它有机/无机化合物的浓度。与表面水因此地下水相互作用有助于为在半干旱地区的水生物种,其中的温度可能以其他方式上升到水平可能是致命的这些物种提供热避难所。随着可持续管理不断增长的需求和利用自然资源,更好地理解生态系统的所有组件,如地下水和地表水之间的联系变得势在必行。这是更相关的半干旱地区环境压力的影响往往更加明显。本文旨在回顾与地表水地下水相互作用的生态水文学的基本概念,并讨论对半干旱地区水资源的可持续管理这种相互作用的相关性refore。

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